In the Atlantic basin, tropical cyclones start in the east and move west until they either reach land or move north into cooler waters.
Based on this map of historic paths, there is a lot of cyclogensis in the east Pacific. However, these paths all end before cyclones reach land, and they also don't curve northward into cooler waters as much as cyclones in the Atlantic basin. So how do they die out? Moreover, why don't cyclones form in warm parts of the central Pacific?